An Assessment of the Erosion Potential of the Fluvial Thermal Process during Ice Breakups of the Lena River (Siberia)
International audience Fluvial thermal erosion following ice breakups of the Lena River (Yakutia, Siberia) is a significant geomorphic process. During the initial stage of ice breakup, ice pushes up onto the river banks and produces large accumulations of ice and sediments that protect the islands...
Published in: | Permafrost and Periglacial Processes |
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Language: | English |
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Online Access: | https://hal.archives-ouvertes.fr/hal-01078016 https://doi.org/10.1002/ppp.1812 |
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ftccsdartic:oai:HAL:hal-01078016v1 2023-05-15T17:07:37+02:00 An Assessment of the Erosion Potential of the Fluvial Thermal Process during Ice Breakups of the Lena River (Siberia) Costard, F. Gautier, E. Fedorov, A. Konstantinov, P. Dupeyrat, L. Géosciences Paris Sud (GEOPS) Université Paris-Sud - Paris 11 (UP11)-Centre National de la Recherche Scientifique (CNRS) Laboratoire de géographie physique : Environnements Quaternaires et Actuels (LGP) Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS) Institut de recherche en astrophysique et planétologie (IRAP) Institut national des sciences de l'Univers (INSU - CNRS)-Université Toulouse III - Paul Sabatier (UT3) Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Observatoire Midi-Pyrénées (OMP) Météo France-Centre National d'Études Spatiales Toulouse (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS) Melnikov Permafrost Institut Russian Academy of Sciences Moscow (RAS) 2014-10-27 https://hal.archives-ouvertes.fr/hal-01078016 https://doi.org/10.1002/ppp.1812 en eng HAL CCSD Wiley info:eu-repo/semantics/altIdentifier/doi/10.1002/ppp.1812 hal-01078016 https://hal.archives-ouvertes.fr/hal-01078016 doi:10.1002/ppp.1812 ISSN: 1045-6740 EISSN: 1099-1530 Permafrost and Periglacial Processes https://hal.archives-ouvertes.fr/hal-01078016 Permafrost and Periglacial Processes, Wiley, 2014, 25 ((3):), pp.162-171 (IF 2,177). ⟨10.1002/ppp.1812⟩ [SDU.STU]Sciences of the Universe [physics]/Earth Sciences info:eu-repo/semantics/article Journal articles 2014 ftccsdartic https://doi.org/10.1002/ppp.1812 2021-10-24T12:53:09Z International audience Fluvial thermal erosion following ice breakups of the Lena River (Yakutia, Siberia) is a significant geomorphic process. During the initial stage of ice breakup, ice pushes up onto the river banks and produces large accumulations of ice and sediments that protect the islands' heads against the mechanical and thermal effects of the river's flow. This initial stage is relatively short and terminates only a few days after breakup begins. In the second phase of flooding, after the river ice has melted, the island heads become free of ice. Hence, when water levels are high, the floodwaters are in sustained contact with the frozen banks of the islands, causing efficient thermal and mechanical erosion of their banks. Such erosion may also occur later in summer, if there is a second discharge peak. Between 2009 and 2012, the retreat of the banks of the river islands displayed high interannual variation that is attributed to the variability of the duration and timing of the flood season. For a given island, the annual rate varied from 2m to 40m and the duration of active thermal erosion of the frozen islands varied from 6 days to 39 days. Copyright (C) 2014 John Wiley & Sons, Ltd. Article in Journal/Newspaper lena river Permafrost and Periglacial Processes Yakutia Siberia Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) River Islands ENVELOPE(-55.765,-55.765,52.317,52.317) Permafrost and Periglacial Processes 25 3 162 171 |
institution |
Open Polar |
collection |
Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
op_collection_id |
ftccsdartic |
language |
English |
topic |
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences |
spellingShingle |
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences Costard, F. Gautier, E. Fedorov, A. Konstantinov, P. Dupeyrat, L. An Assessment of the Erosion Potential of the Fluvial Thermal Process during Ice Breakups of the Lena River (Siberia) |
topic_facet |
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences |
description |
International audience Fluvial thermal erosion following ice breakups of the Lena River (Yakutia, Siberia) is a significant geomorphic process. During the initial stage of ice breakup, ice pushes up onto the river banks and produces large accumulations of ice and sediments that protect the islands' heads against the mechanical and thermal effects of the river's flow. This initial stage is relatively short and terminates only a few days after breakup begins. In the second phase of flooding, after the river ice has melted, the island heads become free of ice. Hence, when water levels are high, the floodwaters are in sustained contact with the frozen banks of the islands, causing efficient thermal and mechanical erosion of their banks. Such erosion may also occur later in summer, if there is a second discharge peak. Between 2009 and 2012, the retreat of the banks of the river islands displayed high interannual variation that is attributed to the variability of the duration and timing of the flood season. For a given island, the annual rate varied from 2m to 40m and the duration of active thermal erosion of the frozen islands varied from 6 days to 39 days. Copyright (C) 2014 John Wiley & Sons, Ltd. |
author2 |
Géosciences Paris Sud (GEOPS) Université Paris-Sud - Paris 11 (UP11)-Centre National de la Recherche Scientifique (CNRS) Laboratoire de géographie physique : Environnements Quaternaires et Actuels (LGP) Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS) Institut de recherche en astrophysique et planétologie (IRAP) Institut national des sciences de l'Univers (INSU - CNRS)-Université Toulouse III - Paul Sabatier (UT3) Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Observatoire Midi-Pyrénées (OMP) Météo France-Centre National d'Études Spatiales Toulouse (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS) Melnikov Permafrost Institut Russian Academy of Sciences Moscow (RAS) |
format |
Article in Journal/Newspaper |
author |
Costard, F. Gautier, E. Fedorov, A. Konstantinov, P. Dupeyrat, L. |
author_facet |
Costard, F. Gautier, E. Fedorov, A. Konstantinov, P. Dupeyrat, L. |
author_sort |
Costard, F. |
title |
An Assessment of the Erosion Potential of the Fluvial Thermal Process during Ice Breakups of the Lena River (Siberia) |
title_short |
An Assessment of the Erosion Potential of the Fluvial Thermal Process during Ice Breakups of the Lena River (Siberia) |
title_full |
An Assessment of the Erosion Potential of the Fluvial Thermal Process during Ice Breakups of the Lena River (Siberia) |
title_fullStr |
An Assessment of the Erosion Potential of the Fluvial Thermal Process during Ice Breakups of the Lena River (Siberia) |
title_full_unstemmed |
An Assessment of the Erosion Potential of the Fluvial Thermal Process during Ice Breakups of the Lena River (Siberia) |
title_sort |
assessment of the erosion potential of the fluvial thermal process during ice breakups of the lena river (siberia) |
publisher |
HAL CCSD |
publishDate |
2014 |
url |
https://hal.archives-ouvertes.fr/hal-01078016 https://doi.org/10.1002/ppp.1812 |
long_lat |
ENVELOPE(-55.765,-55.765,52.317,52.317) |
geographic |
River Islands |
geographic_facet |
River Islands |
genre |
lena river Permafrost and Periglacial Processes Yakutia Siberia |
genre_facet |
lena river Permafrost and Periglacial Processes Yakutia Siberia |
op_source |
ISSN: 1045-6740 EISSN: 1099-1530 Permafrost and Periglacial Processes https://hal.archives-ouvertes.fr/hal-01078016 Permafrost and Periglacial Processes, Wiley, 2014, 25 ((3):), pp.162-171 (IF 2,177). ⟨10.1002/ppp.1812⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1002/ppp.1812 hal-01078016 https://hal.archives-ouvertes.fr/hal-01078016 doi:10.1002/ppp.1812 |
op_doi |
https://doi.org/10.1002/ppp.1812 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
25 |
container_issue |
3 |
container_start_page |
162 |
op_container_end_page |
171 |
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1766063097462652928 |